FASTRAC Thermal Model Analysis By Millan Diaz-Aguado.

Slides:



Advertisements
Similar presentations
Bare rock model Assumptions
Advertisements

Wind Power: For wind power A = frontal area (πr 2 ) m 2 ρ = density of air (≈1.3 kg/m 3 ) v = wind speed Ex – What max power can you get from a wind turbine.
1 MITSUBISHI ELECTRIC CORPORATION PROPRIETARY INFORMATION ANY AND ALL UNAUTHORIZED REPRODUCTION OR DISCLOSURE STRICTLY PROHIBITED IGARSS2011 Development.
1 Space thermal environment Isidoro Martínez 11 July 2008.
Blackbody radiation and solar radiation 1)More on Blackbody Radiation; Black body radiation 2) Magnitude of Solar radiation.
Solar radiation and earth energy balance 1) Paul’s Demo 2) Magnitude of Solar Radiation ( Estimate of the power of Garden lights ) 2) Earth energy balance.
Solar Radiation Emission and Absorption
AAE450 Spring 2009 Slide 1 of 7 Orbital Transfer Vehicle (OTV) Thermal Control Ian Meginnis February 26, 2009 Group Leader - Power Systems Phase Leader.
AAE450 Spring 2009 Kelly Leffel 3/26/09 Structures and Thermal Lunar Descent Phase Lander Integration Lander Thermal Control (Day) Kelly Leffel Structures.
1 Spacecraft Thermal Design Introduction to Space Systems and Spacecraft Design Space Systems Design.
Metal vs. Glass The effect of conduction in baking.
Radiation Heat Transfer. The third method of heat transfer How does heat energy get from the Sun to the Earth? There are no particles between the Sun.
Thermal Modeling of the CX Satellite Jacob Boettcher Thermal Team Lead 4/5/02.
MET 61 1 MET 61 Introduction to Meteorology MET 61 Introduction to Meteorology - Lecture 8 “Radiative Transfer” Dr. Eugene Cordero San Jose State University.
Solar Radiation Emission and Absorption
Presentation by: Heather DeRoy
Radiation Definitions and laws Heat transfer by conduction and convection required the existence of a material medium, either a solid or a.
Pat Arnott, ATMS 749 Atmospheric Radiation Transfer ATMS 749 Atmospheric Radiation Transfer.
What is the Ring of Fire?. Q. What is the Age of Universe? A. About 13.7 billion years (Ga) Q. How do we know this? A. Intensity vs.
Radiative Heat Trade-Offs for Spacecraft Thermal Protection
Thermal Systems Design
NANOSAT THERMAL MANAGEMENT WORKSHOP Sept 2003 Charlotte Gerhart Mechanical Engineer
AAE450 Spring 2009 Kelly Leffel 3/0509 Structures and Thermal Lunar Descent Phase Lander Integration Lander Thermal Control Kelly Leffel Structures and.
Solar Energy Part 1: Resource San Jose State University FX Rongère January 2009.
Energy, Power and Climate Change Formulas. Wind Power.
Lecture 4a. Blackbody Radiation Energy Spectrum of Blackbody Radiation - Rayleigh-Jeans Law - Rayleigh-Jeans Law - Wien’s Law - Wien’s Law - Stefan-Boltzmann.
Lecture 24. Blackbody Radiation (Ch. 7) Two types of bosons: (a)Composite particles which contain an even number of fermions. These number of these particles.
CE 401 Climate Change Science and Engineering solar input, mean energy budget, orbital variations, radiative forcing January 2012.
Thermal Subsystem PDR Josh Stamps Nicole Demandante Robin Hegedus 12/8/2003.
UNIT THREE: Matter, Energy, and Earth  Chapter 8 Matter and Temperature  Chapter 9 Heat  Chapter 10 Properties of Matter  Chapter 11 Earth’s Atmosphere.
Energy, Power and Climate Change Formulas. Wind Power.
Chapter Eleven: Heat 11.1 Heat 11.2 Heat Transfer.
Investigation 9B  Key Question: How is convection responsible for the movement of air through the atmosphere?? Convection in Earth’s Atmosphere.
Conduction and convection require the presence of temperature variations in a material medium. Although radiation originates from matter, its.
Heat Transfer Equations. Fouling Layers of dirt, particles, biological growth, etc. effect resistance to heat transfer We cannot predict fouling factors.
Thermal Subsystem Peer Review Objective: To maintain all components of the space craft within their specific temperature range.
More Radiation EGR 4345 Heat Transfer.
LionSat Thermal Subsystem Team Members: Nathan Hermanson Adam McDonald Joel Thakker.
Energy Balance. HEAT TRANSFER PROCESSES Conductive heat transfer Convective heat transfer Radiation heat transfer.
Science 3360 Lecture 5: The Climate System
Active Solar heating Used for space and or water heating
Thermal Control Subsystem
ESA UNCLASSIFIED – For Official Use FMTM#101: ESATAN-TMS PTSINK - sink temperature data interpretation, Columbus J. Persson Noordwijk 20/11/2015.
1 Atmospheric Radiation – Lecture 9 PHY Lecture 9 Infrared radiation in a cloudy atmosphere.
Wes Ousley June 28, 2001 SuperNova/ Acceleration Probe (SNAP) Thermal.
How much makes it through the atmosphere. Why a seasonal variation? First, why do we have seasons? Earth’s axis is tilted 23.5° to the plane of its orbit.
C osmic R Ay T elescope for the E ffects of R adiation CRaTER Thermal Analysis Huade Tan 6/27/05.
Earth-Sun Relationships The Reasons for the Seasons.
Introduction to On-Orbit Thermal Environments
Introduction to On-Orbit Thermal Environments
Radiation  Solar radiation drives the atmosphere.  The amount of radiation the Earth’s surface and atmosphere receives is dependent on: l The angle at.
Solar Constant Emissivity Albedo
C osmic R Ay T elescope for the E ffects of R adiation CRaTER Pre-Ship Review (I-PSR) Thermal Analysis Christine Cottingham LM/GSFC 545 Hume Peabody GSFC.
Variable e σ  Which is the smaller temperature increment - a degree Celsius or a degree Fahrenheit? Explain.
Rose Navarro HMI Lead Thermal Engineer
Chapter 18. Heat Transfer A PowerPoint Presentation by
The Earth The Earth is the third planet from the Sun.
Radiation.
PRELIMINARY MAP - Sun On Secondary Reflector Analysis #4
Preliminary MAP - Sun On Secondary Reflector Analysis #3
12: Greenhouses and the Earth System
Total energy of particles:
Presentation by: Heather DeRoy
Cold Case Model Hot Case Model GPS LMC GPS LMC Launch
Chapter 18. Heat Transfer A PowerPoint Presentation by
JOSH STAMPS ROBIN HEGEDUS
LRO CRaTER Preliminary Temperature Predictions Design A Concept  Old Concept April 12, 2005 Cynthia Simmons/ESS.
Chapter Eleven: Heat 11.1 Heat 11.2 Heat Transfer.
Conversations with the Earth Tom Burbine
The colour of A star changes depending on it’s temperature
Presentation transcript:

FASTRAC Thermal Model Analysis By Millan Diaz-Aguado

Overview Sun/Shade and Line of Sight Heat Flux (Earth, Albedo, Sun) –Heat Flux Earth and Albedo and View Factor Simple Example (Thin Disk) Two Square Parallel Surfaces –Conduction through the Solar Panel –Radiation to the Structure –Radiation to EMI Future work and Conclusions

Eclipsed vs. Light Find the position of the Sun (Julian Date) and the satellite, and calculate the angle between them (Θ). If θ 1 +θ 2 > Θ then there is Line of Sight

Eclipsed vs. Light Example: i=45º Ω=45º ω=0 h=300km on July 21 st 2005

Environmental Heat Flux Solar Heat Flux ( W/m 2 ) q=1350 α cos(ψ) –Where ψ is the angle between the normal of the spacecraft surface and the Sun and α is the aborptivity of the surface Earth Blackbody Radiation q=σ (T) 4 α F –Where σ is the Stefan-Boltzmann constant, T is the temperature of Earth’s blackbody, and F is the view factor Earth Albedo q=1350 AF α F cos (θ) –Where θ is the angle between the spacecraft surface and the Sun, AF is the Albedo Factor (~at 90 min orbit) Albedo Factor Inclination 0-30 Inclination Inclination Hot Case Cold Case

View Factor Shape factor for different angles between the normal of the surface of the spacecraft and its position vector h/R=0.047 Interpolate data if angle lays between the given data

Heat Flux for a Orbiting Thin Germanium Circular Disk Altitude 300km, i=0º, α = 0.81

Temperature for Thin Disk To calculate the surface temperature we use a simple ODE for radiated thin plate Where ρ is the density, ε is the emissivity, h is the width and T is the temperature of the thin plate

Thermal Model of Two Parallel Plates Plate 1 is facing the Earth Plate 2 is facing away from the Earth Radiation patterns will be different View Factor is different as the plates are square Fse=.98 ε=.85 α=.81 Width=175 μm C=0.093 W-hr/(Kg-°C) ρ=5260 Kg/m³

Surface Heat Flux A) Plate 1 B) Plate 2

Surface Temperatures A) Plate 1B) Plate 2

Conductance Through the Solar Panel 1234 k 12 k 23 k 34 The Solar Panel is assumed to have a multilayer wall The temperature of the inner aluminum surface is calculated by: Where t 1 is the temperature of the outer surface, k is the thermal conductivity, Δx is the thickness and q/A is the heat flux

Radiation Between Two Parallel Surfaces Radiation between the solar panel with side panel and EMI boxes Where T is the surface temperature, ε is the emissivity and σ is the Stefan-Boltzmann 12

Buffed Aluminum Side Panel A) Plate 1B) Plate 2

EMI Golden Anodized Aluminum A) Plate 1B) Plate 2

Conclusion and Future Work Conduction: –Between aluminum side panel and EMI box –Between solar panel and aluminum side panel –Between structural elements Thruster tank Four other sides of the hexagon, top and bottom sides Inner Heat Production –Subsystems and Thruster Rotation of the satellite MLI